28 research outputs found
Spatial characterization of vegetation diversity with satellite remote sensing in the khakea-bray transboundary aquifer
>Magister Scientiae - MScThere have been increasing calls to monitor Groundwater-Dependent Ecosystems (GDEs) more effectively, since they are biodiversity hotspots that provide several ecosystem services. The accurate monitoring of GDEs is an indispensable under Sustainable Development Goal (SDG) 15, because it promotes the existence of phreatophytes. It is imperative to monitoring GDEs, since their ecological significance (e.g., as biodiversity hotspots) is not well understood in most environments they exist. For example, vegetation diversity in GDEs requires routine monitoring, to conserve their biodiversity status and to preserve the ecosystem services in these environments. Such monitoring requires robust measures and techniques, particularly in arid environments threatened by groundwater over–abstraction, landcover and climate change. Although in–situ methods are reliable, they are challenging to use in extensive transboundary groundwater resources such as the Khakea-Bray Transboundary Aquifer
Biodiversity of Angola
This open access multi-authored book presents a 'state of the science' synthesis of knowledge on the biodiversity of Angola, based on sources in peer-reviewed journals, in books and where appropriate, unpublished official reports. The book identifies Angola as one of the most biologically diverse countries in Africa, but notes that its fauna, flora, habitats and the processes that drive the dynamics of its ecosystems are still very poorly researched and documented. This 'state of the science' synthesis is for the use of all students of Angola's biodiversity, and for those responsible for the planning, development and sustainable management of the country's living resources. The volume brings together the results of expeditions and research undertaken in Angola since the late eighteenth century, with emphasis on work conducted in the four decades since Angola's independence in 1975. The individual chapters have been written by leaders in their fields, and reviewed by peers familiar with the region
Biodiversity of Angola
This open access multi-authored book presents a 'state of the science' synthesis of knowledge on the biodiversity of Angola, based on sources in peer-reviewed journals, in books and where appropriate, unpublished official reports. The book identifies Angola as one of the most biologically diverse countries in Africa, but notes that its fauna, flora, habitats and the processes that drive the dynamics of its ecosystems are still very poorly researched and documented. This 'state of the science' synthesis is for the use of all students of Angola's biodiversity, and for those responsible for the planning, development and sustainable management of the country's living resources. The volume brings together the results of expeditions and research undertaken in Angola since the late eighteenth century, with emphasis on work conducted in the four decades since Angola's independence in 1975. The individual chapters have been written by leaders in their fields, and reviewed by peers familiar with the region
Mapping benthic ecological diversity and interactions with bottom-contact fishing on the Flemish Cap (northwest Atlantic)
Versión del editor2,69
Protected Area Management
Until recently, values and benefits from protected areas have often been underestimated as well as taken for granted. Protected Area Management - Recent Advances demonstrates that there are deep necessities in how the wider scientific, environmental, socioeconomic, and cultural values that these natural ecosystems provide should increasingly be recognized. The book highlights various approaches for managing and conserving protected areas to respond to some pressing global challenges such as climate change, demand for food and energy, overexploitation, and habitat change. It addresses these issues in five main sections that cover biodiversity and genetic resources; protected marine areas; community, ecotourism, and protected areas; and protected area conservation and monitoring
Biodiversity: ecosystem function relationships in southern African woodlands
A broad corpus of previous research has sought to understand the role of
biodiversity as a driver of ecosystem structure and function. Although theory
suggests that increased biodiversity should increase ecosystem function by
niche complementarity among co-existing species, in natural systems wide
variation in the biodiversity effect exists among vegetation types and along
environmental gradients. In southern African woodlands and savannas, which
experience disturbance by fire and herbivory, drought and extreme temperatures,
it is unclear whether positive biodiversity effects should occur. In this thesis,
I explore the ecology of southern African woodlands through the lens of the
biodiversity-ecosystem function relationship, to improve our understanding of
the role of tree diversity as a mediator of ecosystem function, its interactions
with abiotic environment, and its effect on woodland structure.
In temperate and wet tropical forests, where the majority of biodiversity-ecosystem function studies in natural woody vegetation have been conducted,
the positive effect of niche complementarity hinges on the condition that conspecific competition is the limiting factor to ecosystem function. In highly disturbed
and environmentally stressed systems however, this may not hold true. I conducted a regional study investigating the role of tree species diversity and structural
diversity as mediators of woody biomass, using a plot network of 1235 plots
spanning wide climatic and biogeographic gradients across southern Africa.
Using Structural Equation Modelling, I determined that tree species diversity
has a positive effect on biomass, operating mostly via its effect on structural
diversity. I found that biodiversity itself increases with water availability, and that
positive biodiversity effects only arise under sufficiently high stem density.
To further understand the ecological mechanisms which drive positive
biodiversity-productivity relationships, I explored the effects of tree species
diversity and woodland demographic structure on patterns of land-surface phenology. I combined a dense plot-based tree census dataset across multiple
deciduous Zambian woodland types with remotely sensed measures of greenness, to understand drivers of variation in pre-rain green-up, growing season
length and productivity. I found that pre-rain green-up occurred earlier in more
diverse sites, across all woodland types, while in non-miombo woodlands, species richness also increased post-rain senescence lag and season length. I also
found that large-sized trees increase the degree of both pre-rain green-up and
post-rain senescence lag, across vegetation types, with an effect size similar to
that of species richness.
Southern African woodlands occur as a complex mosaic of open grassy
patches and closed canopy forest-like patches, driven by positive feedbacks of
fire-induced tree mortality and grass growth, but the biotic mechanisms causing
variation in canopy closure are unclear. I used terrestrial LiDAR at two sites, in
Tanzania and Angola, to understand at fine spatial scale the effects of species
composition and diversity on canopy architecture and canopy cover. Species
diversity was found to allow increased spatial clumping of trees, which drove
vertical canopy layer diversity and canopy height, demonstrating an indirect role
of species diversity on canopy cover via stand structure. Taken together with
the regional study of the biodiversity-ecosystem function relationship, these
findings suggest a nuanced role of tree species diversity on ecosystem function,
operating primarily via its effect on canopy structural diversity in southern
African woodlands. I propose that higher diversity communities are more likely
to produce forest-like closed canopy woodlands, with a higher upper limit on
biomass, and are more likely to transition from savanna to closed canopy forest
under conditions of atmospheric CO2 enrichment.
Finally, in an effort to increase our understanding of the variation in diversity
and structure of woodlands across southern Africa, I conducted a study of tree
species biodiversity and woodland structure in Bicuar National Park, southwest
Angola, with comparison to other woodlands around the miombo ecoregion.
Much of the published plot data and woodland monitoring infrastructure in
miombo woodlands is located in central and eastern regions of southern Africa,
while woodlands in the west of the region, which occur entirely within Angola,
remain poorly represented. I found that Bicuar National Park constitutes an
important woodland refuge at the transition between dry miombo woodland
and Baikiaea-Baphia woodlands. I recorded 27 tree species not recorded
elsewhere in the miombo ecoregion outside the HuÃla plateau. An additional
study of one-off plots in areas previously disturbed by shifting cultivation, found
that this disturbance increases tree species diversity, but ultimately reduces
woody biomass, even after a period of regeneration, potentially representing a
directional shift to a different stable vegetation type.
Together, the findings of this thesis demonstrate multiple relationships among
tree biodiversity, ecosystem structure, and ecosystem function, measured
primarily through woody biomass and productivity, at multiple spatial scales.
I conclude that incorporation of diversity and canopy structural information
into earth system models, by scaling up plot data using cutting edge remotely
sensed datasets, could improve predictions of how climate change and biodiversity change will impact the functioning of different vegetation types across
southern Africa, with consequences for carbon cycle modelling, conservation
management, and ecosystem service provision. Finally, I suggest that biodiversity loss of large archetypal miombo tree species will have the greatest
impact on a number of ecosystem functions related to carbon cycling, raising
concerns over the impacts of selective logging of these species
Climate variability and extremes in the Okavango River Basin, southern Africa
The Okavango River Basin (ORB) located in southern Africa is a region of highly sensitive and biodiverse ecosystems. It spans Angola, Namibia and Botswana, with the world-famous Okavango Delta located in the latter country. The ecosystems depend on the highly seasonal ORB streamflow, which is also the major source of freshwater for the rural population, most of whom depend on subsistence farming. Climate variability and extremes such as droughts, hot days and extreme rainfall events are not well understood over this region. Also, the relationship between climate and other aspects like vegetation and river discharge are not well understood. To contribute to a better understanding of this relationship, the thesis investigated relationships between rainfall, temperature, Normalized Difference Vegetation Index (NDVI) and river discharge, and their interannual variability and trends. It was found that at monthly and seasonal time scales, NDVI spatial patterns are closely related to those of rainfall than temperature. The NDVI-rainfall and NDVI-temperature relationships differ north of 18.9°S where rainfall is higher than to its south. Correlations between NDVI and rainfall show lags of 1-2-months. Large areas across the region show significant warming trends in all seasons but mainly in October-December (OND), as well as wetting mainly in the north. The warming trend may imply more evaporation and desiccation which may exacerbate extreme event impacts such as severe droughts. Interannual variability of rainfall, NDVI and temperature is pronounced with significant correlations with El Niño-Southern Oscillation (ENSO), the subtropical Indian Ocean Dipole (SIOD) and the Botswana High for rainfall and temperature, and for NDVI with ENSO. The temperature (rainfall) correlations with ENSO and the Botswana were positive (negative), with the SIOD they were negative (positive), and the NDVI-ENSO correlations were negative. On longer time scales, the wet 2006-2013 period was analysed relative to much drier 1999-2005 epoch for OND. The 2006-2013 wetter conditions appear linked to La Niña Modoki conditions, regional circulation differences and warmer sea surface temperature near Angola. Extreme rainfall events over the ORB were analysed. The analysis was performed within a larger region in western central southern Africa (WCSA), given that many rainfall events extend beyond river basin boundaries. Focus was placed on extreme rainfall events accumulated over 1-day (DP1) and 3-days (DP3), during the main rainy season, January-April (JFMA). Due to data sparsity, the Climate Hazards Group Infrared Precipitation with Station data (CHIRPS) were used to identify these events. It was found that contributions of DP1 and DP3 events to JFMA rainfall totals are, on average, ~10% and ~17%, respectively, but in some years their contributions exceed 30%. Most of the events result from tropical-extratropical cloud bands, with tropical lows being also important. Interannual variability in extreme events is substantial and appears linked to ENSO and the Botswana High. Although ENSO influences the extreme events and rainfall totals more generally over southern Africa, by far the neutral JFMA 2017 season experienced the wettest conditions over the world-famous Okavango Delta region. Factors that contributed to these heavy rains included a deeper Angola Low, weaker mid-level Botswana High and anomalous westerly moisture fluxes from the tropical southeast Atlantic during January – early March. The second most intense rainfall event occurred on April 22nd, resulting from a cut-off low. DP1 frequencies show significant increasing trends, and similarly, rain-days and rain totals over many areas. These trends have important implications for agricultural and water management as well as wildlife conservation in the ORB. To contribute to a better understanding of drought over the ORB region, the thesis analysed various drought metrics. These include a Cumulative Drought Intensity (CDI) index, based on the product of maximum dry spell duration and maximum temperature anomaly, and the Standardised Precipitation-Evapotranspiration Index (SPEI). Strong horizontal gradients in frequencies of dry spells and hot days were found to shift south over the ORB from August to November as the tropical rain-belt shifts increasingly south of the equator, the Congo Air Boundary declines and the Botswana High strengthens and shifts south-westwards. By December, the tropical gradient in dry spell frequencies is unnoticeable while that across the Limpopo River and southern ORB region, where the Botswana High is centred, stands out. On seasonal time scales, October-November 2013-2021 is particularly hot and dry over the Okavango Delta region. The thesis provided evidence that this hot and dry epoch is related to a stronger and southward shifted Botswana High and reduced low-level moisture convergence. On interannual time scales, there were strong relationships with the Botswana High, and to lesser extent ENSO. A strong drying-warming trend was found in the early summer, linked to a significant strengthening of the Botswana High. These trends, in conjunction with the Coupled Model Intercomparison Project Phase 6 (CMIP6) projected early summer drying over southern Africa found in the literature, may impact severely on the sensitive ecosystems of the ORB, and on water availability as well as subsistence farming in the region
Impact of climate change on vegetative species diversity in Masvingo Province, Zimbabwe
Vegetative species diversity is under threat from environmental pressures, particularly climate
change. As the impacts of climate change vary from place to place, response of vegetative
species diversity to a changing climate also vary depending on geographical location. The
response of vegetative species diversity under dry conditions in Zimbabwe is not well known.
This study assessed the impact of climate change on vegetative species diversity under semiarid
conditions of Masvingo province in Zimbabwe. This was achieved by determining climate
change trends over a period of forty years (1974-2014), and examining the relationship between
vegetative species diversity and spatially interpolated climate data. The absence of historical
diversity data prompted the use of remote sensing to enable the assessment of spatial and
temporal changes. Thus, the Normalised difference vegetation index (NDVI) was used to
assess vegetative species diversity changes after establishing a positive relationship between
species diversity and NDVI. The mixed methods research design was used as the strategy of
inquiry. The non-aligned block sampling design was used as the sampling framework from
which 198 sampling points were identified. Meteorological data obtained from Zimbabwe
Meteorological Services Department (ZMSD) and the National Climate Data Centre (NCDC)
were used for climate change analysis. Data collected through image analysis, direct
observations, questionnaire surveys and interviews were used to assess the impact of climate
change on vegetative species diversity. Results indicate that all temperature and precipitation
variables have significant (p<0.05) trends over the period under study. However, the trend for
seasonal total precipitation was not significant but declining. The significant trends indicate
that climate change occurred over the period under study. 93% of the respondents confirmed
having experienced the climate change phenomenon. Results also show a significant
relationship between climate elements (precipitation and temperature) and vegetative species
diversity represented by Shannon Weaver Index (H). More so, there is a positive relationship
between NDVI and H. Vegetative species diversity represented by NDVI decreased over the
period under review. The results indicate that climate change has contributed to the decrease
of vegetative species diversity in Masvingo province, thus it is a force behind many other
factors contributing to biodiversity loss.College of Agriculture and Environmental SciencesPh. D. (Environmental Sciences